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相关概念视频

Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Thermosensation01:43

Thermosensation

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Peripheral thermosensation is the perception of external temperature. A change in temperature (on the surface of the skin and other tissues) is detected by a family of temperature-sensitive ion channels called Transient Receptor Potential, or TRP, receptors. These receptors are located on free nerve endings. Those detecting cold temperatures are closer to the surface of the skin than the nerve endings detecting warmth. These thermoTRP channels, while temperature selective, have relatively...
30.4K
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
12.4K
Sublimation01:03

Sublimation

739
Sublimation is the direct transformation of a solid to a gaseous state. For instance, at standard pressure and room temperature, solid carbon dioxide sublimes to gaseous carbon dioxide. The phase diagram depicts the conditions required for sublimation. This process occurs at the solid-gas phase boundary and is not observed above the triple point of the substance. The reverse of sublimation is called deposition, where a gaseous substance condenses directly into a solid. Sublimation and...
739
Heating and Cooling Curves02:44

Heating and Cooling Curves

22.9K
When a substance—isolated from its environment—is subjected to heat changes, corresponding changes in temperature and phase of the substance is observed; this is graphically represented by heating and cooling curves.
For instance, the addition of heat raises the temperature of a solid; the amount of heat absorbed depends on the heat capacity of the solid (q = mcsolidΔT). According to thermochemistry, the relation between the amount of heat absorbed or released by a substance, q, and its...
22.9K
Mechanisms of Heat Transfer I01:14

Mechanisms of Heat Transfer I

4.3K
Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.
4.3K

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相关实验视频

Updated: Jul 4, 2025

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
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Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

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热与冷的降温启动开始.

Zhong-Hai Li1

  • 1Key Laboratory of Computational Geodynamics, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, China.

National science review
|January 30, 2024
PubMed
概括
此摘要是机器生成的。

新的潜伏区以两种不同的方式开始,形成热或冷道. 这些独特的初始潜水道导致了对比的地质记录,为板块构造学提供了洞察力.

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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System
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Evolution of Staircase Structures in Diffusive Convection
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相关实验视频

Last Updated: Jul 4, 2025

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System
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科学领域:

  • 地质地质地质地质地质地
  • 构造学 构造学 构造学 构造学
  • 地球科学 地球科学 地球科学

背景情况:

  • 俯冲区是板块构造学的关键特征.
  • 潜伏的启动阶段是复杂的,并未完全理解.
  • 不同的启动机制可能导致不同的地质结果.

研究的目的:

  • 探索新的潜伏区启动的两个主要模式.
  • 为了区分热和冷的初始沉降道.
  • 了解由这些不同的启动路径产生的对比的地质记录.

主要方法:

  • 地质建模地质建模
  • 对地震数据的分析.
  • 从活跃边缘进行现场观测的比较.

主要成果:

  • 已经确定了两种不同的潜水启动路径:热和冷.
  • 热通道与特定的岩和变态特征有关.
  • 寒冷通道表现出不同的热和结构特性,导致独特的地质记录.

结论:

  • 俯冲区的启动机制显著影响其早期演变.
  • 了解这些对比的路径是解释过去潜水事件的地质记录的关键.
  • 这项研究为区分热和冷初始潜水带提供了一个框架.